Seasonal Variability in Mercury’s Calcium Exosphere Matthew Burger Morgan State University/GESTAR Rosemary Killen (NASA/GSFC) Bill McClintock (U. Colorado/LASP) Ronald Vervack, Jr. (JHU APL) Menelaos Sarantos (UMBC) Tim Cassidy (U. Colorado/LASP) Aimee Merkel (U. Colorado/LASP)
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Seasonal Variability in Mercury’s Calcium Exosphere Matthew Burger Morgan State University/GESTAR Rosemary Killen (NASA/GSFC) Bill McClintock (U. Colorado/LASP)
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• All the calcium comes from a small region on the surface near the dawn, equatorial point
• Comes off very hot (T>20,000 K)
• Source size and temperature don’t change much over 8 Mercury Years
• Source strength varies
with Mercury’s
distance from the sun
Burger et al. (2012)
Dawn SourceIsotropic Source
We Don’t Know Why• Not related to the surface geology
•Source is fixed in local time and does not rotate with Mercury
• Not related to the magnetosphere (ion sputtering or electron stimulated desorption)•Magnetosphere is highly variable•Wouldn’t produce a source at dawn
• Possibly related to asymmetric impact vaporization•But not clear why only Ca shows this dawn source
• Not related to Ca freezing on the nightside and vaporizing as it moves into sunlight
Terminator Motion
I0 vs Terminator Speed
H vs Terminator Speed
Fits at 6 am (dawn)
Sun moves backwards in sky
Summary• Calcium comes off the surface very hot from a small
region near dawn•The source has been stable for eight Mercury years
• The source mechanism is still unknown•We are using numerical models of the physics that we do understand to figure out what we don’t understand.